Slide 1Riccardo Zei ICRC 2007 (Merida - Messico) OG 1.1CREAM-II C & O Spectra
Preliminary measurements of carbon and oxygenenergy spectra from the second flight of CREAM
Riccardo Zei(University of Siena & INFN)
for the CREAM Collaboration
30th International Cosmic Ray Conference - Merida, Mexico, 3 — 11 July 2007
Slide 2Riccardo Zei ICRC 2007 (Merida - Messico) OG 1.1CREAM-II C & O Spectra
H.S. Ahn1, O. Ganel1, J.H. Han1, K.C. Kim1, M.H. Lee1, A. Malinin1,E.S. Seo1,2, R. Sina1, P. Walpole1, J. Wu1, Y.S.Yoon1,2, S.Y. Zinn1
1 Institute for Physical Science and Technology, University of Maryland, College Park, MD 20742, USA2 Department of Physics, University of Maryland, College Park, MD 20742, USA
N.B. Conklin, S. Coutu, S.I. MognetDepartment of Physics, Penn State University, University Park, PA 16802, USA
P.S. Allison, J.J. Beatty, T.J. BrandtDepartment of Physics, Ohio State University, Columbus, OH 43210, USA
J.T. Childers, M.A. DuvernoisSchool of Physics and astronomy, University of Minnesota, Minneapolis, MN 55455, USA
M.G. Bagliesi, G. Bigongiari, P. Maestro, P.S. Marrocchesi, R. ZeiDepartment of Physics, University of Siena & INFN, Via Roma 56, 53100 Siena, Italy
J.A. Jeon, S. Nam, I.H. Park, N.H. Park, J. YangDepartment of Physics, Ewha Womans University, Seoul 120-750, Republic of Korea
S. MinnickDepartment of Physics, Kent State University, Tuscarawas, New Philadelphia, OH 44663, USA
S. NutterDepartment of Physics, Northern Kentucky University, Highland Height, KY 41099, USA
L. BarbierAstroparticle Physics Labroratory, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA
Slide 3Riccardo Zei ICRC 2007 (Merida - Messico) OG 1.1CREAM-II C & O Spectra
CREAM-II trajectory
For the present analysis, only a subset of CREAM-II data was selected
Altitude 38—40 km. Average atmospheric overburden ~ 3.9 g/cm²
CREAM flightsCREAM-I: 2004/05 campaign•Total flight time ~ 42 days~ 42M science events collected
CREAM-II: 2005/06 campaign•Total flight time ~ 28 days•~ 27M science events collected
Record breaking flight
Effective Live Time ~ 17 days
Slide 4Riccardo Zei ICRC 2007 (Merida - Messico) OG 1.1CREAM-II C & O Spectra
Instrument configuration (2nd flight)
Timing Charge Detector (TCD)• scintillator paddles (2 charge measurements)
• backscatter rejection by fast pulse shaping
Cherenkov Detector (CD)• acrylic radiator (charge measurement)
• vetoes low energy particles
Silicon Charge Detector (SCD)• 2 layers of Si pixels (2 charge measurements)
• backscatter rejection by fine segmentation
Target (T1,T2)• 19 cm densified Graphite (~ 0.5 λint , ~ 1 X0)
• induces a hadronic interaction
Tungsten Sci-Fi Calorimeter (CAL)• 20 X0; 1 cm granularity (energy measurement)
Slide 5Riccardo Zei ICRC 2007 (Merida - Messico) OG 1.1CREAM-II C & O Spectra
Silicon Charge Detector (SCD)• 2 layers of sensors
• 380 μm thick Si sensor
• 16 pixels per sensor
• pixel size ~ 2.1 cm2
• 2496 channels/layer were readout
• No dead area between sensors
• Active area per layer ~ 0.52 m2
• particle-ID by charge measurement from Z=1 to Z=33
Slide 6Riccardo Zei ICRC 2007 (Merida - Messico) OG 1.1CREAM-II C & O Spectra
Tungsten Sci-Fi Calorimeter• Active area 50x50 cm2
• Longitudinal sampling: 3.5 mm W (1 X0) + 0.5 mm Sci-Fi
• Transverse granularity: 1 cm (20 fibers ~ 1 Moliere radius)
• Total of 20 layers (20 X0 , ~ 0.7 λint): alternate X-Y views
• 2560 channels (3 gain ranges) readout by 40 HPDs
Tungsten Sci-Fi Calorimeter
Optical fibers
Slide 7Riccardo Zei ICRC 2007 (Merida - Messico) OG 1.1CREAM-II C & O Spectra
Geometric Factor
Monte Carlo Generation: FLUKA 2005.6 with hadronic interaction package DMPJET-3
Carbon (Oxygen) nuclei isotropic generation according to power-law spectrum in the energy range 600 (800) GeV – 100 TeV Accepted incoming particle
Geometrical Acceptance is calculated selecting events crossing both SCD Top Plane and CAL Top Layer
Selected fiducial region:SCD top plane side = 78 cmCAL top plane side = 50 cm
GF ~ 0.46 m2 sr
Rejected incoming particle
Slide 8Riccardo Zei ICRC 2007 (Merida - Messico) OG 1.1CREAM-II C & O Spectra
Shower reconstruction & Charge-ID
• Shower imaging (lateral/longitudinal) with CAL
• Fit of the shower axis
• Back-projection of CAL track to SCD
• The track is matched with the SCD pixel hit by the incoming particle
• Rejection of backscattered particles
• Charge identification of the incoming particle (a consistent charge assignement from the 2 layers is required)
Slide 9Riccardo Zei ICRC 2007 (Merida - Messico) OG 1.1CREAM-II C & O Spectra
Observed charge distribution in SCD
0.7 1.3Top
Bottom
SS
≤ ≤Consistency 30% cut:
2Re 2
( )Top Bottomc
S SZ
+∝
Carbon & Oxygen: σ ~ 0.2e
O
N
C
pathlength correction applied
• Indicative of charge resolution
• NOT representative of elemental abundances
Slide 10Riccardo Zei ICRC 2007 (Merida - Messico) OG 1.1CREAM-II C & O Spectra
Charge Reconstruction Efficiency (Monte Carlo)
• Charge Reconstruction Efficiency is normalized to the number of triggered events
• MC algorithm for charge identification with SCD is the same as applied on flight data
• Preliminary MC estimate of charge reconstruction efficiency is ~ 70% (above 2 TeV) including effects of SCD masked sensors
Carbon
Oxygen
Slide 11Riccardo Zei ICRC 2007 (Merida - Messico) OG 1.1CREAM-II C & O Spectra
Flight DATA: carbon and oxygen energy deposit in CAL
All reconstructed showers inside selected fiducial region 39390
After Consistency cut for SCD signals 10890
Nuclei Charge Selection 728 (Oxygen)
583 (Carbon)
Carbon Oxygen
Slide 12Riccardo Zei ICRC 2007 (Merida - Messico) OG 1.1CREAM-II C & O Spectra
For events surviving the selection cuts,both distributions of energy deposit and primary particle energy are divided into equidistant logarithmic bins.
Through their correlation plot, we can
estimate the matrix elements Aij i.e. the probability that events in the deposited energy bin icome from the primary incident energy bin j.
Energy Deconvolution
( ) ( , ) ( )d dE A E E E dEϕ = Φ∫Deposited energy
Primary energy
A(Ed,E) is determined from Monte Carlo events
Response function
Slide 13Riccardo Zei ICRC 2007 (Merida - Messico) OG 1.1CREAM-II C & O Spectra
Correction to TOI (Top of Instrument): Interaction fractions
Correction to TOA (Top of Atmosphere)
Through MC simulation the correction factor η is calculated foran (average) residual atmosphere overburden of ~ 3.9 g/cm2.
Carbon = 0.86 Oxygen = 0.83
• A correction for particles interacting in the instrument was applied.
Fraction of Carbon/Oxygen nuclei interacting in the apparatus
Slide 14Riccardo Zei ICRC 2007 (Merida - Messico) OG 1.1CREAM-II C & O Spectra
Absolute Flux
The unfolded counts Ninc, in each incident energy bin of size ∆E, are normalized to obtain the absolute differential fluxes at the top of atmosphere, given by
1( )inc
F l
NEE G T ε η
Φ = ×Δ ⋅ ⋅ ⋅
where
GF = Geometric factorTl = Live-timeε = product of efficiencies , correction for interaction fractionsη = TOA correction
Slide 15Riccardo Zei ICRC 2007 (Merida - Messico) OG 1.1CREAM-II C & O Spectra
Preliminary Carbon & Oxygen energy spectra
Slide 16Riccardo Zei ICRC 2007 (Merida - Messico) OG 1.1CREAM-II C & O Spectra
Conclusions
Thanks to:• NASA
• NSBF/CSBF
• INFN/PNRA
• WFF
• NSF
• A preliminary analysis of the data indicates an excellent charge-ID from SCD and good performance of the imaging calorimeter and of the whole instrument
• Preliminary carbon and oxygen energy spectra are found to be consistent with previous measurements
• Analysis is on-going... more to come!